Astronomy Exam 3

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276 Terms

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Earth's layers (outside to in)
Crust, mantle (hot solid rock that slowly convects), liquid outer core (iron/nickel), solid inner core (iron/nickel)
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Differentiation
Dense material sinks to the center and lighter material rises, forming layers (core, mantle, crust)
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P waves (pressure)
Compressional seismic waves; travel through solids AND liquids; faster
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S waves (shear)
Seismic waves that travel only through solids; slower; blocked by Earth's liquid outer core
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How do we know Earth's outer core is liquid?
S waves are blocked by it (shadow zone) and P waves bend as they pass through
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What causes Earth's magnetic field?
A dynamo: convection of the liquid metallic outer core plus Earth's rotation
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Earth's magnetic field characteristics
Roughly dipolar, tilted slightly from the rotation axis, reverses occasionally; forms the magnetosphere that deflects the solar wind
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Aurora
Charged solar-wind particles funneled by the magnetic field toward the poles hit atmospheric oxygen and nitrogen, making them glow; more frequent near sunspot maximum and after CMEs
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What does a planetary magnetic field imply?
A liquid, conducting, convecting interior plus rotation
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Plate tectonics
Lithosphere is broken into plates that move a few cm/year, driven by mantle convection
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Rift (divergent) zone
Plates move apart and new crust forms (mid-ocean ridges, East African Rift)
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Subduction (convergent) zone
One plate dives beneath another, producing trenches, volcanoes, and earthquakes; colliding continents make mountains
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Transform boundary
Plates slide past each other (San Andreas Fault)
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Continental drift (Wegener)
Continents were once joined (Pangaea); evidence: matching coastlines, fossils, and rock types across oceans
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Where is volcanic activity on Earth concentrated?
Mostly along the borders of tectonic plates
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Atmosphere layers (bottom to top)
Troposphere (weather), stratosphere (ozone), mesosphere, thermosphere (auroras), exosphere
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Major constituents of Earth's atmosphere
About 78% nitrogen, 21% oxygen, about 1% argon, trace CO2 and water vapor
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Greenhouse effect
Surface re-radiates infrared; gases like CO2, water vapor, and methane absorb it and re-emit it downward, warming the planet
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Why is the greenhouse effect important?
Without it Earth would be well below freezing; it makes life possible
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Why are fossil fuels a concern?
Burning them adds CO2 that strengthens the greenhouse effect and drives global warming
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Major driver of global climate change
Buildup of CO2 and other greenhouse gases (NOT ozone)
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Other planet with an extreme greenhouse effect
Venus (runaway greenhouse effect)
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Ozone layer
Stratospheric O3 that absorbs harmful ultraviolet light
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CFCs
Refrigerant/aerosol chemicals that release chlorine, destroying ozone (the ozone hole); banned by the Montreal Protocol
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Lunar maria
Dark smooth plains; ancient lowland basins filled with lava billions of years ago (not oceans)
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Lunar highlands
Bright, old, heavily cratered terrain
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Regolith (lunar dust)
Fine powdery soil produced by billions of years of impacts breaking up surface rock
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Why does the Moon preserve so many craters?
No atmosphere, no weather or erosion, and little geologic activity
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Near side vs. far side of the Moon
Near side has large maria; far side is mostly heavily cratered highlands because its crust is thicker so lava rarely reached the surface; both get equal sunlight
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Does the Moon have an atmosphere?
Essentially none (too little gravity)
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Does the Moon have a magnetic field?
None today (small, mostly solid core)
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Why do we always see the same side of the Moon?
Synchronous rotation: it rotates once per orbit
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Moon vs. Earth density
Moon is less dense (small iron core)
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Water ice on the Moon
Found in permanently shadowed polar craters, probably delivered by comets; does NOT mean liquid water once covered the surface
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Co-accretion theory (Moon)
Earth and Moon formed together; problem: Moon lacks an iron core and has a different density/composition
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Capture theory (Moon)
Moon formed elsewhere and was captured; problem: hard gravitationally, and Moon rocks match Earth's mantle isotopically
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Fission theory (Moon)
Fast-spinning young Earth flung off the Moon; problem: Earth could not spin fast enough and angular momentum is wrong
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Giant impact (collision-ejection) theory
A Mars-sized body (Theia) hit the young Earth and the debris formed the Moon; the currently accepted theory
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Why is the giant impact theory accepted?
Explains the Moon's small iron core and low density, rocks matching Earth's mantle, early molten surface, and the system's angular momentum
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Terrestrial planets
Mercury, Venus, Earth, Mars
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Terrestrial planets by size (largest to smallest)
Earth, Venus, Mars, Mercury
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Smallest planet
Mercury
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Densest planet
Earth
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Hottest planet
Venus (about 460 C, runaway greenhouse)
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Which terrestrial planets have moons?
Earth (1) and Mars (2: Phobos and Deimos); Mercury and Venus have none
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Which terrestrial planets rotate slowly?
Mercury (3 rotations per 2 orbits) and Venus
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Which planet rotates backward (retrograde)?
Venus (very slowly; its day is longer than its year)
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Mercury features
Cratered like the Moon, little or no maria, almost no atmosphere, weak magnetic field, scarps from planetary shrinking
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Scarps on Mercury
Cliffs showing the planet shrank as its core cooled long after formation
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Venus atmosphere
Very thick CO2 (about 90x Earth's pressure) with sulfuric acid clouds
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Venus surface age
Only a few hundred million years old (from crater counts); global resurfacing by volcanism
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Why did Magellan use radar at Venus?
Thick clouds block visible light; radar passes through them
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Does Venus have a magnetic field?
No (no strong global field)
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Mars atmosphere
Thin, low-density CO2; low pressure; temperatures vary with seasons
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Olympus Mons
Tallest volcano/mountain in the solar system; on Mars
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Valles Marineris
Huge canyon system on Mars
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Percival Lowell's Martian canals
An optical illusion
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How do we know some meteorites came from Mars?
Gases trapped in the rock match Mars's atmosphere
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Which planets could possibly sustain life?
Earth (certainly) and Mars (possibly past or microbial); Venus is too hot
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Why is Mars better than Venus for colonization?
Moderate temperatures, thin atmosphere (not crushing), water ice, Earth-like day, solid surface; needs thicker atmosphere, oxygen, radiation protection, and water
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Jovian (giant) planets
Jupiter, Saturn, Uranus, Neptune
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Largest planet
Jupiter
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Smallest giant planet
Neptune (slightly smaller than Uranus in diameter)
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Least dense planet
Saturn (would float)
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Which planet has an extremely tilted axis (about 98 degrees)?
Uranus (extreme seasons)
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Which giants have liquid metallic hydrogen?
Jupiter and Saturn; it produces their strong magnetic fields
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Ice giants
Uranus and Neptune
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Giant planet atmospheres are dominated by
Hydrogen (then helium), plus methane, ammonia, and water compounds
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Giant planet storms
Larger and longer-lived than on terrestrials (Great Red Spot, Great Dark Spot)
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Internal heat of giant planets
Jupiter, Saturn, and Neptune radiate as much or more energy from internal convection as they get from the Sun
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Planet with the longest orbit
Neptune (not Uranus)
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Which planets have rings?
All four giants; Saturn's are the most spectacular
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Saturn's rings are made of
Billions of small objects in orbit, made of ice and rock
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Voyager 2
Flew past Uranus (1986) and Neptune (1989); never landed
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Io
Jupiter's moon; most volcanically active body; active lava volcanoes powered by tidal heating
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Europa
Jupiter's moon; ice crust over a subsurface liquid water ocean; top candidate for life
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Ganymede
Jupiter's moon; largest moon in the solar system; own magnetic field; probable subsurface ocean
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Callisto
Jupiter's moon; heavily cratered ancient surface; possible subsurface ocean
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Titan
Saturn's moon; thick nitrogen atmosphere, methane/ethane lakes and seas; Huygens landed here
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Enceladus
Saturn's moon; water geysers from the south pole; subsurface ocean; candidate for life
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Triton
Neptune's moon; retrograde orbit (probably captured Kuiper Belt object); nitrogen geysers
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Which moons might support life?
Europa and Ganymede (Jupiter), Enceladus and Titan (Saturn); liquid water or hydrocarbons, energy (tidal heating), organic chemistry
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Exoplanet detection methods
Transit (star dims) and radial velocity (stellar wobble); also direct imaging and microlensing
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Hot Jupiters
Giant planets very close to their stars; explained by planetary migration
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Crater counting
More craters means an older surface; gives relative ages
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Radioactive dating
Uses decay of radioactive isotopes to give absolute ages
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Age of the solar system
About 4.5 billion years, from radioactive dating of primitive meteorites
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Solar nebula theory step 1
A cloud of gas and dust (solar nebula) collapses under gravity
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Conservation of angular momentum (nebula)
As the cloud shrinks it spins faster and flattens into a disk
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Protosun
Dense hot center of the nebula that begins fusion and becomes the Sun
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Condensation
Solids form from cooling gas; only metal and rock inside the frost line, ices too beyond it
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Accretion
Early process in which colliding particles stick together and grow
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Planetesimals
Small bodies formed by accretion that merge into protoplanets
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Why do giant planets have H and He?
They grew large (aided by ices beyond the frost line) and could capture gas; terrestrials could not
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Why did terrestrial planets form close to the Sun?
Only metal and rock could condense there; these are scarce so the planets stayed small (NOT because rock was more plentiful)
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Evidence for the solar nebula theory
Coplanar same-direction orbits, same-direction spins, composition trends, disks around young stars, meteorite ages
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Problems for the solar nebula theory
Hot Jupiters, Uranus's tilt, Venus's retrograde rotation, origin of the Moon
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Why are Earth-like worlds differentiated?
Continuing impacts on a growing protoplanet melted the entire body
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Which solid worlds stay geologically active longest?
The largest (they retain heat best)
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How was the Sun's distance determined?
Radar ranging and Kepler's laws (the Astronomical Unit)